Major types and characteristics of Late Paleozoic ore deposits, East Tianshan, northwest China | |
Han CM(韩春明); Han, CM; Zhao, GC | |
刊名 | INTERNATIONAL GEOLOGY REVIEW |
2003 | |
卷号 | 45期号:9页码:798-813 |
通讯作者 | Chinese Acad Sci, Inst High Energy Phys, Beijing, Peoples R China ; Univ Hong Kong, Dept Earth Sci, Hong Kong, Hong Kong, Peoples R China |
英文摘要 | One of the largest and most important metallogenic provinces in China is the East Tianshan, where seven major types of Late Palcozoic metal deposits have been recognized: (1) porphyry-type Cu-Mo-(Au) ore; (2) volcanic Fe-Cu; (3) orogenic lode gold; (4) magmatic Cu-Ni sulfide; (5) epithermal gold; (6) volcanic hydrothermal Cu; and (7) skarn Cu-Ag. Tectonically, the development of these Late Paleozoic mineral deposits was closely associated with subduction and closure of the ancient Tianshan ocean, lying between the Tarim craton and the Junggar-Kazakhstan composite block. In Late Devonian to Early Carboniferous time, the northern edge of the Tarim craton existed as a passive continental margin, whereas the ancient Tianshan oceanic crust was subducted beneath the southern margin of the Junggar-Kazakhstan block, resulting in the formation of the Dananhu-Tousuquan magmatic are and associated porphyry-type Cu-Mo-(Au) deposits. In Middle Carboniferous time, the ancient Tianshan oceanic crust began to subduct beneath the northern margin of the Tarim craton, leading to the formation of the Aqishan-Yamansu magmatic arc and associated volcanic Fe-Cu deposits. In the Late Carboniferous, the ancient Tianshan ocean closed, and a continent-arc collision occurred, leading to the formation of the Tianshan orogen. Following collision, an extensional event, associated with the emplacement of voluminous ultramafic-mafic complexes and formation of a number of large- to medium-scale magmatic copper-nickel ore deposits, occurred along the Kangger suture zone. In Early Permian time, East Tianshan entered into a post-collision stage associated with widespread emplacement of granitoid bodies and within-plate volcanism, which led to the formation of hydrothermal copper deposits, skarn-type Cu-Ag deposits, post-orogenic gold deposits, and epithermal gold deposits. |
学科主题 | Geology |
类目[WOS] | Geology |
研究领域[WOS] | Geology |
原文出处 | SCI |
语种 | 英语 |
WOS记录号 | WOS:000185729300003 |
内容类型 | 期刊论文 |
源URL | [http://ir.ihep.ac.cn/handle/311005/238514] |
专题 | 高能物理研究所_加速器中心 |
作者单位 | 中国科学院高能物理研究所 |
推荐引用方式 GB/T 7714 | Han CM,Han, CM,Zhao, GC. Major types and characteristics of Late Paleozoic ore deposits, East Tianshan, northwest China[J]. INTERNATIONAL GEOLOGY REVIEW,2003,45(9):798-813. |
APA | 韩春明,Han, CM,&Zhao, GC.(2003).Major types and characteristics of Late Paleozoic ore deposits, East Tianshan, northwest China.INTERNATIONAL GEOLOGY REVIEW,45(9),798-813. |
MLA | 韩春明,et al."Major types and characteristics of Late Paleozoic ore deposits, East Tianshan, northwest China".INTERNATIONAL GEOLOGY REVIEW 45.9(2003):798-813. |
个性服务 |
查看访问统计 |
相关权益政策 |
暂无数据 |
收藏/分享 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。
修改评论